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Canepa's Car Wash(Pacific Avenue) <br /> Problem Assessment Report and Corrective Action Plan <br /> Page 4 <br /> On September 20, break through on the second carbon unit effluent was measured by PID at 2 parts per <br /> million by volume. The carbon in the first vessel was replace and the piping rerouted so the new carbon <br /> is in the second vessel in series. The system was restarted on September 30, 2002. <br /> In the Report — Soil and Groundwater Investigation, dated June 12, 1998, Condor recommended <br />' additional soil and groundwater investigation to further characterize the extent of contamination at the <br /> site. Condor performed additional groundwater investigation at the site consisting of three CPT borings, <br /> hydropunch sampling, and the installation of three soil borings and four monitor wells. Details of the <br /> investigation are presented in the Additional Soil and Groundwater Investigation Report dated January <br /> 21, 2002. Twelve monitor wells, MW-1 through MW-12d, were surveyed as part of the investigation. The <br /> new survey identified errors in the previously reported elevations of monitor wells MW-6 and MW-7. The <br />' new survey elevations for these wells are higher than previously reported, and consequently, the <br /> groundwater elevation contours for the site no longer indicated a groundwater mound in the vicinity of <br /> well MW-2. The task of surveying the monitor wells was sufficient to complete the Groundwater <br /> Mounding Study Report dated February 13, 2002. <br />' Soil samples were collected immediately above the groundwater in selected wells and soil borings during <br /> the investigation described in the January 21, 2002 report. The purpose of those soil samples was to <br />' evaluate existing vadose zone contamination. No contaminants were detected in the vadose zone. <br /> In August 2001, Condor conducted a sensitive receptor survey within a 2,000-foot radius of the site to <br /> identify potential areas of groundwater recharge or discharge (surface water bodies), schools, and <br /> potential water well users that could be impacted by migration of groundwater from the site. The results <br /> • of the sensitive receptor survey are included in the Quarterly Groundwater Monitoring (Third Quarter <br />' 2001) and Sensitive Receptor Survey Report, dated August 16, 2001. The results indicated the presence of <br /> several domestic and municipal wells, two schools, three child-care facilities, and three leaking <br /> underground storage tank (LUST) sites within the study area. No actively pumped drinking water wells <br />' were identified within 500 feet of the site, however. <br /> Condor performed quarterly monitoring at the site on January 10, 2002 and April 10, 2002. Laboratory <br /> analytical results of the groundwater samples indicated concentrations of petroleum hydrocarbon <br /> constituents that were consistent with historical data. The analytical results also indicated substantial <br /> declines in contaminant concentration in monitor wells MW-11 and MW-12d compared to the initial <br /> sampling results. <br />' 4.0 HYDROGEOLOGY <br />' The car wash site is situated on fine-grained flood plain deposits overlying distal alluvial fan deposits <br /> sloping westward from the eastern part of San Joaquin County. The upper part (-50 to 60 feet) of the <br /> section underlying the site is made up of flood-stage, overbank deposits consisting mostly of clay, clay- <br /> rich silt, and silt. Following retreat of the flood waters, the muds and silts dry out and desiccation cracks <br /> Corm. Ahiindnnt vegetation may also c.nver the flood plain. Interbedded with the overbank deposits are <br /> less abundant clayey-, silty-, and poorly-sorted sands that may have originated as channel or natural levee <br /> deposits. The interbedded sandy deposits appear to be thin and may be discontinuous. <br /> Generalized geological sections have been constructed from the boring logs for the site monitor wells and <br /> soil borings. The sections are shown in Figures 3, 4, and 5. In general, black to gray organic clay is <br /> present from the surface to about eight feet. Beneath the clay to a depth of about 50 to 60 feet are silt <br /> • deposits with interbedded and discontinuous lenses of clayey to silty sand. Root molds and carbonate <br /> �� CONDOR <br />